Dust Over Strait of Hormuz and Gulf of Oman

Dust blows off the coast of Iran and over the Strait of Hormuz and the Gulf of Oman. In winter in this region, dust storms are associated chiefly with the passage of westerly depressions. Here, the dust storm may be connected to a local phenomenon known as the “Shamal” (an Arabic word for “north”).

A shamal is defined as sustained winds of 25 knots or greater. Wind direction is almost always northwesterly. The Shamal produces the most widespread hazardous weather known to the region. The winter Shamal is generally characterized by durations of either 24-36 hours or 3-5 days.

This “3-5 Day Shamal” occurs 1-3 times a winter and produces the strongest winds and highest seas found in the Persian Gulf. Over exposed Persian Gulf waters, sustained winds have reached 50kt which have produced 15+ ft seas. The 3-5 day shamal arises from the temporary stagnation of a 500mb short wave over or just east of the Strait of Hormuz , or from the establishment of a mean long wave trough stalling approximately 56E. Persistent dust and sandstorms occur.

Dust that restricts visibility is confined to the coasts and the immediate offshore areas of the Gulf of Oman during a strong “Shamal”. Visibility drops as low as 3-5NM. Worst conditions are found at the mouths of rivers or canyons. Dust settles rapidly once winds drop below 15kt.